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Biomineralization of Poorly Crystalline Fe(III) Oxides by Dissimilatory Metal Reducing Bacteria (DMRB)

Zachara, John M., Kukkadapu, Ravi K., Fredrickson, James K., Gorby, Yuri A., Smith, Steven C.·2002·Geomicrobiology Journal
DOI 10.1080/01490450252864271
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Abstract

Dissimilatory metal reducing bacteria (DMRB) catalyze the reduction of Fe(III) to Fe(II) in anoxic soils, sediments, and groundwater. Two-line ferrihydrite is a bioavailable Fe(III) oxide form that is exploited by DMRB as a terminal electron acceptor. A wide variety of biomineralization products result from the interaction of DMRB with 2-line ferrihydrite. Here we describe the state of knowledge on the biotransformation of synthetic 2-line ferrihydrite by laboratory cultures of DMRB using select published data and new experimental results. A facultative DMRB is emphasized ( Shewanella putrefaciens ) upon which most of this work has been performed. Key factors controlling the identity of the secondary mineral suite are evaluated including medium composition, electron donor and acceptor concentrations, ferrihydrite aging/recrystallization status, sorbed ions, and co-associated crystalline Fe(III) oxides. It is shown that crystalline ferric (goethite, hematite, lepidocrocite), ferrous (siderite, vivianite), and mixed valence (magnetite, green rust) iron solids are formed in anoxic, circumneutral DMRB incubations. Some products are well rationalized based on thermodynamic considerations, but others appear to result from kinetic pathways driven by ions that inhibit interfacial electron transfer or the precipitation of select phases. The primary factor controlling the nature of the secondary mineral suite appears to be the Fe(II) supply rate and magnitude, and its surface reaction…

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Crossref · 10.1080/01490450252864271

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  • Many factors contribute to formation of specific Fe(II)-bearing secondary minerals as products of dissimilatory iron reduction, including Fe(III) oxide mineralogy, particle aggregation, rate and extent of Fe(II) production, electron shuttles, DIRB species and population size, oxyanions, dissolved NOM, and electron donor concentration and type.

    “Many factors have been identified as contributing to the formation of specific Fe(II)-bearing secondary minerals as products of DIR, including Fe(III) oxide mineralogy, [20,35]; Fe(III) oxide particle aggregation, [41]; the rate and extent of Fe(II) production, [33,35,42,43]; the presence of electron shuttles, [33]; the species and population size of the DIRB, [44][45][46]; the presence of oxyanio”

    From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [42]

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Metadata

Authors
Zachara, J. M., Kukkadapu, R. K., Fredrickson, J. K., Gorby, Y. A., & Smith, S. C.
Venue
Geomicrobiology Journal
Publisher
Informa UK Limited
Published
2002-03
Volume
19
Issue
2
Pages
179-207
ISSN
  • 0149-0451
  • 1521-0529
DOI
10.1080/01490450252864271
Cited by
364
References
1
Language
en

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